First – Rocky Mountain National Park is open year round, 24 hours a day. So no worries there. However, if you want to drive Trail Ridge Road, you need to visit from around the end of May to early October. July through September are the busiest time of year, so my recommendation to avoid the crowds and still get good weather, plus plenty of light for activities, would be June.
Cow Creek Trail follows Cow Creek, with its many beaver ponds, extending past the Bridal Falls turnoff as the Dark Mountain trail, then joining the Black Canyon trail to intersect the Lawn Lake trail shortly below the lake. North Boundary Trail connects to the Lost Lake trail system. North Fork Trail begins outside of the park in the Comanche Peak Wilderness before reaching the park boundary and ending at Lost Lake. Stormy Peaks Trail connects Colorado State University's Pingree Park campus in the Comanche Peak Wilderness and the North Fork Trail inside the park.
Below 9,400 feet (2,865 m), temperatures are often moderate, although nighttime temperatures are cool, as is typical of mountain weather. Spring comes to the montane area by early May, when wildflowers begin to bloom. Spring weather is subject to unpredictable changes in temperature and precipitation, with potential for snow along trails through May. In July and August, temperatures are generally in the 70s or 80s °F during the day, and as low as the 40s °F at night. Lower elevations receive rain as most of their summer precipitation.
The land at Dao House sits on what was once a gathering place of peace for rival Native American tribes in the region. Over the years, it has operated as a homestead, a ranch and a fox farm before becoming a lodge for the first time in 1948. In 2015, Dao House emerged as a meeting point of western and eastern cultures and today, they offer lodging, equestrian experiences and wellness activities including an oxygen lounge, internal martial arts, personalized retreat programs and shorter wellness getaways.
Glacial geology in Rocky Mountain National Park can be seen from the mountain peaks to the valley floors. Ice is a powerful sculptor of this natural environment and large masses of moving ice are the most powerful tools. Telltale marks of giant glaciers can be seen all throughout the park. Streams and glaciations during the Quaternary period cut through the older sediment, creating mesa tops and alluvial plains, and revealing the present Rocky Mountains. The glaciation removed as much as 5,000 feet (1,500 m) of sedimentary rocks from earlier inland sea deposits. This erosion exposed the basement rock of the Ancestral Rockies. Evidence of the uplifting and erosion can be found on the way to Rocky Mountain National Park in the hogbacks of the Front Range foothills. Many sedimentary rocks from the Paleozoic and Mesozoic eras exist in the basins surrounding the park.
Fall River Village: Located along the banks of Fall River and the popular Riverwalk, Fall River Village is Estes Park’s newest and best located resort. Situated on six and a half acres of beautiful mountain landscape, the resort features 60 new two bedroom, two bath vacation condos. The resort has an in-ground, outdoor pool and year-round, outdoor hot tub, a community room, fire pit and grill areas, and an outdoor recreation area with yard games and a hammock. Perfect for friends and family to gather together for memories that will last a lifetime.
Estes Park is the gateway into the national park, but it’s also a destination unto itself. Stop by The Barrel, a seasonal alfresco beer garden, and window-shop along Elkhorn Ave., Estes' bustling main thoroughfare. Filled with one-of-a-kind stores, several fine restaurants and plenty of places for an afternoon snack, the area is just steps from the park’s eastern entrance. Stop for coffee and sit outside on the Riverwalk.
Lawn Lake Trail climbs to Lawn Lake and Crystal Lake, one of the parks deepest lakes, in the alpine ecosystem and along the course of the Roaring River. The river shows the massive damage caused by a dam failure in 1982 that claimed the lives of three campers. The trail is a strenuous snowshoe hike in the winter. Ypsilon Lake Trail leads to its namesake as well as Chipmunk Lake, with views of Longs Peak, while traversing pine forests with grouseberry and bearberry bushes. The trail also offers views of the canyon gouged out by rampaging water that broke loose from Lawn Lake Dam in 1982. Visible is the south face of Ypsilon Mountain, with its Y shaped gash rising sharply from the shoreline.